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    Supercooling at the Surface of an Arctic Lead

    Source: Journal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 004::page 482
    Author:
    Katsaros, Kristina B.
    DOI: 10.1175/1520-0485(1973)003<0482:SATSOA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Supercooling of the surface water on open leads in the Arctic Ocean has been suggested as a possible source of water for the observed subsurface freezing. Observations with an infrared radiometer at the shore-lead outside Pt. Barrow, Alaska, in April 1972, verify this supposition.
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      Supercooling at the Surface of an Arctic Lead

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162182
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    contributor authorKatsaros, Kristina B.
    date accessioned2017-06-09T14:43:47Z
    date available2017-06-09T14:43:47Z
    date copyright1973/10/01
    date issued1973
    identifier issn0022-3670
    identifier otherams-25402.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162182
    description abstractSupercooling of the surface water on open leads in the Arctic Ocean has been suggested as a possible source of water for the observed subsurface freezing. Observations with an infrared radiometer at the shore-lead outside Pt. Barrow, Alaska, in April 1972, verify this supposition.
    publisherAmerican Meteorological Society
    titleSupercooling at the Surface of an Arctic Lead
    typeJournal Paper
    journal volume3
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1973)003<0482:SATSOA>2.0.CO;2
    journal fristpage482
    journal lastpage486
    treeJournal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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